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Copy file name to clipboardExpand all lines: docs/_sources/configuration_file.rst.txt
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@@ -38,14 +38,14 @@ The following input lines in the configuration file are:
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12#If cartesian, number of z cells [-]; if tensor, variable array of z-refinment; if corner-point, fix array of z-refinment (17 entries)
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70. 36.25 #Temperature bottom and top rig [C]
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19620000. #Pressure on the top [Pa]
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1e-92e-8#CO2 diffusion (in liquid and gas) [m^2/s]
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1e-92e-80#Diffusion (in liquid and gas) [m^2/s] and dispersion [m] (disperison only available in Flow master)
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8.5e-12500. #Rock specific heat and density (for spe11b/c)
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5e41. #Pore volume on lateral boundaries and width of buffer cell [m] (for spe11b/c)
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150. 10. #Elevation of the parabola and back [m] (for spe11c)
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In line 5 you specify if you are using OPM Flow from the master branch or from the latest stable release (OPM-flow 2023.4 release).
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This since there are continuous changues in the OPM master branch (e.g., the format of the boundary condition keyword BC). Then we
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will keep updating the decks for using Flow from master and also we will keep the framework to produce decks compatible for the latest OPM stable release.
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In line 5 you specify if you are using OPM Flow from the master branch or from the latest stable release (OPM-flow 2023.10 release).
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This since there are continuous changues in the OPM master branch (e.g., implementation of mechanical dispersion). Then we
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will keep updating the decks for using Flow from master and also we will keep the framework to produce decks compatible for the latest OPM stable release.
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The immiscible model allows for faster prototyping while the complete model includes dissolution of the components in the
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gas and liquid phases, in addition to thermal effects. Regarding the grid type, the cartesian mode generates an uniform grid
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with the defined number of elements in lines 9 to 11. The tensor grid allows to define arrays in each direction where the grid
@@ -63,6 +63,10 @@ resulting in 17 levels. Then, the z-refinment in each of these levels is set. Se
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elements, the tensor grid by setting the x-array to 50,100,20; the y-array to 5,10,70,10,5; and the z-array to 5,10,20,20,20,20,20,5; and
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the corner-point grid using the same xy-arrays as in the tensor grid and for the z-refinment 4,4,3,3,5,3,7,5,13,5,7,5,3,9,21,21,2.
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.. warning::
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Dispersion seems to work fine for the spe11a case where there are no thermal effects nor water evaporation. However, for spe11b/c there are
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issues with the current implementation (we are working in this, then for now disperison should be set to 0 for spe11b/c).
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***********************
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Soil-related parameters
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***********************
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PERM4506.625PORO40.20THCONR41.25
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PERM51013.25PORO50.25THCONR50.92
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PERM62026.50PORO60.35THCONR60.26
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PERM70PORO70THCONR72.00
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PERM70PORO71E-6THCONR72.00
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.. figure:: figs/kr.png
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.. figure:: figs/cap.png
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Visualization in ResInsight of the relative permeability and capillary pressure functions in the facie 1.
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.. note::
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For spe11b/c, adding a small value of porosity in facie 7 (i.e., 1E-6 in this example), allows to include the termal effects
<spanclass="linenos">11</span><spanclass="mi">12</span><spanclass="c1">#If cartesian, number of z cells [-]; if tensor, variable array of z-refinment; if corner-point, fix array of z-refinment (17 entries)</span>
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<spanclass="linenos">12</span><spanclass="mf">70.</span><spanclass="mf">36.25</span><spanclass="c1">#Temperature bottom and top rig [C]</span>
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<spanclass="linenos">13</span><spanclass="mf">19620000.</span><spanclass="c1">#Pressure on the top [Pa]</span>
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<spanclass="linenos">14</span><spanclass="mf">1e-9</span><spanclass="mf">2e-8</span><spanclass="c1">#CO2 diffusion (in liquid and gas) [m^2/s]</span>
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<spanclass="linenos">14</span><spanclass="mf">1e-9</span><spanclass="mf">2e-8</span><spanclass="mi">0</span><spanclass="c1">#Diffusion (in liquid and gas) [m^2/s] and dispersion [m] (disperison only available in Flow master)</span>
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<spanclass="linenos">15</span><spanclass="mf">8.5e-1</span><spanclass="mf">2500.</span><spanclass="c1">#Rock specific heat and density (for spe11b/c)</span>
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<spanclass="linenos">16</span><spanclass="mf">5e4</span><spanclass="mf">1.</span><spanclass="c1">#Pore volume on lateral boundaries and width of buffer cell [m] (for spe11b/c)</span>
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<spanclass="linenos">17</span><spanclass="mf">150.</span><spanclass="mf">10.</span><spanclass="c1">#Elevation of the parabola and back [m] (for spe11c)</span>
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</pre></div>
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</div>
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<p>In line 5 you specify if you are using OPM Flow from the master branch or from the latest stable release (OPM-flow 2023.4 release).
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This since there are continuous changues in the OPM master branch (e.g., the format of the boundary condition keyword BC). Then we
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will keep updating the decks for using Flow from master and also we will keep the framework to produce decks compatible for the latest OPM stable release.
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<p>In line 5 you specify if you are using OPM Flow from the master branch or from the latest stable release (OPM-flow 2023.10 release).
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This since there are continuous changues in the OPM master branch (e.g., implementation of mechanical dispersion). Then we
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+
will keep updating the decks for using Flow from master and also we will keep the framework to produce decks compatible for the latest OPM stable release.
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The immiscible model allows for faster prototyping while the complete model includes dissolution of the components in the
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gas and liquid phases, in addition to thermal effects. Regarding the grid type, the cartesian mode generates an uniform grid
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with the defined number of elements in lines 9 to 11. The tensor grid allows to define arrays in each direction where the grid
the corner-point grid using the same xy-arrays as in the tensor grid and for the z-refinment 4,4,3,3,5,3,7,5,13,5,7,5,3,9,21,21,2.</span><aclass="headerlink" href="#id1" title="Link to this image"></a></p>
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</figcaption>
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</figure>
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<divclass="admonition warning">
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<pclass="admonition-title">Warning</p>
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<p>Dispersion seems to work fine for the spe11a case where there are no thermal effects nor water evaporation. However, for spe11b/c there are
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issues with the current implementation (we are working in this, then for now disperison should be set to 0 for spe11b/c).</p>
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</div>
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</section>
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<sectionid="soil-related-parameters">
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<h2>Soil-related parameters<aclass="headerlink" href="#soil-related-parameters" title="Link to this heading"></a></h2>
<p><spanclass="caption-text">Visualization in ResInsight of the relative permeability and capillary pressure functions in the facie 1.</span><aclass="headerlink" href="#id2" title="Link to this image"></a></p>
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</figcaption>
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</figure>
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<divclass="admonition note">
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<pclass="admonition-title">Note</p>
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<p>For spe11b/c, adding a small value of porosity in facie 7 (i.e., 1E-6 in this example), allows to include the termal effects
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from the caprock (facie 7).</p>
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</div>
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</section>
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<sectionid="well-related-parameters">
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<h2>Well-related parameters<aclass="headerlink" href="#well-related-parameters" title="Link to this heading"></a></h2>
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